Sure thing! For Buffalo Lake effect generally occurs on the backside of a high pressure system this late in the season when arctic air blows over the relatively warm air lake water. The term fetch (direction and distance the cold air travels over the lakes. The greater the distance the more intense the snow band) not only determines the location of the snow band but the intensity as well.
Lake enhanced is generally when a frontal boundary transits over the lakes and continues to destabilize due to the warm waters. This enhances the storm total snowfall.
In summary, lake creates snow independent of a frontal boundary by cold winds blowing over warm water, while lake enhanced causes systems to become stronger and dump more snow.
please let me know if I didn’t explain well and I’ll try a different approach.